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Detrital chromian spinels from the Sa Kaeo-Chanthaburi accretionary complex, eastern Thailand : tectonic evolution of the western margin of Indochina

机译:泰国东部Sa Kaeo-Chanthaburi增生复合体的碎屑铬铁尖晶石:印度支那西缘的构造演化

摘要

The geological evidence regarding the origin and tectonic setting of eastern Thailand now still be limited. In this study, I studied a melange terrane in the Sa Kaeo-Chanthaburi area, and discriminated tectono-stratigraphic units there. To establish the tectonic evolution , the geochemistry of chromian spinels is applied to determine the composition and provenance of their ultramafic-mafic rocks. Two kinds of rock assemblages are generally recognized in the Sa Kaeo-Chanthaburi area. They are a various kind of melanges, and turbidite deposits. These rock assemblages are called here as the Sa Kaeo-Chanthaburi accretionary complex. It comprises five new rock units from north to south, Khao Prik, Khao Hleam, Ban Nong Bon and Soi Dao units, and Pong Nam Ron Formation. The covering sediments, Pong Nam Ron sandstones belong to the dissected arc. In this Sa Kaeo-Chanthaburi accretionary complex, numerous detrital chromian spinels are discovered as the accessory mineral in turbiditic sandstones of the Pong Nam Ron Formation, sandstone blocks in melanges, and volcaniclastic rocks. The petrographical characteristics under the microscope indicate volcanic origins. Geochemistry the detrial chromian spinels from sandstone beds of the Pong Nam Ron Formation and sandstone blocks in melange have wider Cr content. On the other hand, detrital spinels from volcaniclastic rock have high Cr content, and vary widely in TiO2 content. The Fe3+ is consistently low in both clastic and volcaniclastic rocks. Based upon provenance discrimination fields on the Fe3+/(Cr+Al+Fe3+)-TiO2 diagram proposed by Arai (1992), plots of detrial chromian spinels in sandstones of the Pong Nam Ron Formation and sandstone blocks in melanges seem to correspond to island-arc region, whereas plots of detrital chromian spinels in volcaniclastic rock can be related with spinels from intraplate basalt and island arc basalt. ・・・
机译:关于泰国东部的起源和构造环境的地质证据现在仍然有限。在这项研究中,我研究了Sa Kaeo-Chanthaburi地区的一个混杂地层,并区分了该地区的构造地层单元。为了建立构造演化,运用铬铁尖晶石的地球化学来确定其超镁铁质-镁铁质岩石的成分和物源。 Sa Kaeo-Chanthaburi地区通常公认两种岩石组合。它们是各种混杂物和浊石沉积物。这些岩石组合在这里称为Sa Kaeo-Chanthaburi增生复合物。它包括从北到南的五个新岩石单元,Khao Prik,Khao Hleam,Ban Nong Bon和Soi Dao单元以及Pong Nam Ron组。覆盖的沉积物,Pong Nam Ron砂岩属于解剖弧。在这个Sa Kaeo-Chanthaburi增生复合物中,发现了大量碎屑铬尖晶石,作为Pong Nam Ron组的浊积砂岩,混杂岩中的砂岩块和火山碎屑岩的辅助矿物。显微镜下的岩石学特征表明了火山的起源。地球化学Pong Nam Ron组砂岩中的有害铬铁尖晶石和混杂岩中的砂岩块具有较宽的Cr含量。另一方面,来自火山碎屑岩的碎屑尖晶石具有较高的Cr含量,并且TiO 2含量变化很大。在碎屑岩和火山碎屑岩中,Fe3 +含量始终较低。根据Arai(1992)提出的Fe3 + /(Cr + Al + Fe3 +)-TiO2图上的物源辨别场,Pong Nam Ron组砂岩中的碎铬尖晶石图和混杂岩中的砂岩块似乎对应于弧区,而碎屑铬铁尖晶石在火山碎屑岩中的分布可能与板内玄武岩和岛弧玄武岩的尖晶石有关。 ・ ・ ・

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    Chutakositkanon Vichai;

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  • 年度 2004
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